ASTR 121 (O'Connell) Study Guide 20
Jupiter from Voyager with Io and Europa in foreground
"And now for something completely
different," as they used to say on Monty Python.
The Jovian planets (Jupiter, Saturn, Uranus, and Neptune) are
entirely unlike the terrestrial planets. They may have rocky
cores, like larger versions of the Earth, at their centers, but these
are enveloped in giant gaseous atmospheres. Only the outermost skins
of these atmospheres can be studied directly. This is
meteorology, instead of the geology/topography we discussed for
the terrestrials. However, it can be just as extreme with respect to
Earth-bound meteorology as are the canyons and mountains of Mars
compared to those of Earth.
Another major distinction of the Jovians is the large number of
satellites they possess. The satellites, observed at close range by
spacecraft, exhibit an astonishing diversity of surface types and
features. Unlike the three terrestrial planet satellites, the larger
Jovian satellites are rich in water ice and exhibit many different
phenomena as a consequence. In many ways, they are more interesting
than their parent planets. They may even harbor biospheres. The ring
systems of the Jovians are probably the remnants of distintegrated
satellites.
Many examples of a third kind of planet have recently been
discovered outside the orbit of Neptune. These are perhaps most aptly
called the "ice dwarfs," of which Pluto is the archetype.
A. HISTORY
Prehistory: Jupiter, Saturn known
1600's: Telescopic studies show satellites of J & S, red spot of J,
rings of S
1781: Herschel
discovers Uranus (accidental)---first new planet in recorded
history
1790+: Deviations in U orbit, assumed caused by gravity of
unknown planet, lead to prediction of its location based on Newton's law
of gravity.
1845: Neptune discovered as predicted = a
triumph of Newtonian mechanics
1930:
Tombaugh discovers Pluto. Much more difficult than Neptune.
1950+: Deeper searches: no planet larger than Neptune to 60 AU's
1979-89: Voyager 1 & 2 spacecraft fly by J, S, U, N. Highly successful
missions, but require elaborate planning.
1992: First KBO object (other than Pluto) discovered.
1994: Comet Shoemaker-Levy 9 collides with Jupiter; acts as
an atmospheric probe.
1995: Galileo orbiter/probe mission arrives at Jupiter; sends
probe ~ 50 miles into atmosphere; orbiter continues to study
J. and satellites
2000: On its way to Saturn, the Cassini-Huygens mission passed close
to Jupiter in order to pick up a velocity boost from Jupiter's
gravity. Obtained images, magnetic field, and other measures of
Jupiter.
2004: Cassini-Huygens mission enters orbit around Saturn.
2005: Huygens probe lands safely on Saturn's largest satellite, Titan.
2006: International Astronomical Union debate over the status of Pluto
and other KBO's. Pluto redefined as "dwarf planet."
B. JOVIAN PLANETS (J,S,U,N): PROPERTIES
These four share gross properties. Pluto is entirely different (see
below).
Distant from Sun: 5-30 AU. (Pluto is at 39 AU.) The outer solar system is
vast (over 10,000 times the volume of the inner solar system out to
Mars) and sparsely populated.
Large: 4-11 x Earth radius. Masses 15(U)-318(J) x Earth. J. contains
twice as much mass as all other planets combined. An animated
image of Jupiter's rotation is shown at the right.
Jupiter is midway (on a power of ten scale) between planets and stars. Objects
only 13 times more massive are considered to be small stars.
Structures
- Internal
structures are entirely different from terrestrial planets. A
product of their formation out of the cool regions of the solar nebula,
dominated by icy (H-rich) solids.
- Low mean density (~ 1 gr/cc) ===> mainly composed of H, He; only small
rocky cores. U,N have larger complements of heavy elements than J,S.
- High internal pressures in J,S convert hydrogen to liquid "metallic"
form in their interiors
Visible Surfaces
- No solid surfaces: these are "gas giants"
- Visible surfaces = cloud layers, about 150 miles deep. Clouds
consist of 3 main types of ice crystals: ammonia, ammonium hydrosulfide,
water. Colors are from trace compounds. Thin, white clouds on
Neptune are methane crystals.
- "Spots", e.g. Jupiter's Red Spot (large oval in image above right:
22,000 mi long ~ 3x Earth). Long-lived cyclonic storms. Similar
features on other planets (e.g. the transient "Great Dark Spot" on Neptune).
- Banding (see Saturn image in pseudocolor, below right)
caused by lateral winds and rising/falling convection
currents. Winds reach 300-600 mph on J,S; maximum of
1300 mph on Neptune.
Videos of Jupiter atmosphere:
Special Probes of Jupiter
Magnetic Fields: strong; generated by motions in liquid
metallic hydrogen interior in J,S; produce strong radiation belts,
up to 100x Earth's
Pseudo-color infrared image of
Saturn
C. RING SYSTEMS
Saturn system is brightest, but rings are present around all 4 Jovians
- Not solid: the inner rings rotate faster than the outer
ones, as expected for objects in Keplerian gravitational orbits
- Composed of billions of ice-coated particles (typically about 10 cm in
size). Different particle sizes, coatings produce some of the
structure visible in the rings.
- Origin: debris from tidally/collisionally fragmented
satellites
Rings lie inside the planet's Roche Limit. Inside the RL,
gravity tides would pull apart a large body, such as a satellite.
- Structure: complex! (at right). The biggest gaps are "resonance"
effects produced by the cyclical gravitational tug of the satellites
outside the ring. The ringlets may be produced by the self-gravity
of the material in the rings.
Video of Saturn's rings
D. JOVIAN PLANET SATELLITES
Numerous: 8-63
Click here for Java animation of orbits of
satellites
Diverse(!) characteristics; often violent histories
Larger moons are mixtures of rocky/icy materials
- 3 as large as Mercury
- Form with planet
Smaller sats irregular in shape
- Many are captured rocky or icy planetesimals
Interesting examples:
- Io
(J) (at right): continual volcanic eruptions caused by heating
from tidal flexing in Jupiter's gravitational field. Much more active
today than Venus or Mars. Click for enlargement.
- Europa (J):
ice-coated; new evidence from Galileo orbiter of underlying
oceans (kept warm by tidal flexing?). There is much
speculation about a possible biosphere on Europa (see Study Guide 23).
- Titan
(S): has a thick
atmosphere!---mostly nitrogen with small amount of
methane. Photo-chemistry has produced many hydrocarbons that form an
obscuring haze. For atmospheric profile, click
here.
Titan is a main target of the Cassini-Huygens
Mission. While the primary spacecraft stays in orbit around
Saturn, the Huygens probe was detached and successfully landed on Titan's surface in
January 2005, relaying data during its descent and for a short period
on the ground.
Recent radar data from the primary Cassini spacecraft shows that there
are large lakes
on Titan, probably of methane or ethane.
- Miranda (U): shattering
collision & reassembly? or surface scars from internal convection?
- Enceladus(S) and
Triton (N): water/ice geysers; plume
from Enceladus feeds Saturn's "E ring"
Artist's Concept of Huygens Probe at Titan
E. PLUTO AND THE KUIPER BELT
Pluto is entirely unlike the other four large outer planets. It is smaller by a factor of 2 than
any of the other 8 planets.
It is a rocky/icy object rather than a gas giant.
When first discovered, Pluto was thought to be isolated at the edge of
the Solar System. However, in the last 15 years, astronomers have
discovered many more such bodies, some with
sizes comparable to Pluto. These are all members of the "Kuiper
Belt".
- The Kuiper Belt is a huge volume beyond the orbit of Neptune, centered on
the ecliptic plane, but extending many AU's above and below the
plane. Over 1000 "Kuiper Belt Objects" (KBOs) have been discovered in
this volume to date.
- The largest known KBO---yes, it's bigger than
Pluto---is Eris, renamed and categorized as a dwarf planet in
2006. It is estimated to be 2400 km in diameter (Pluto is only
2300 km). Click here for a page describing Eris by its discoverer, Mike Brown.
- Sedna;
discovered March 2004 is, at 90 AU, most distant identified member of Solar System;
highly elliptical orbit, perihelion 75 AU; period 10,500 years; lies beyond
the Kuiper Belt.
These discoveries precipitated the messy discussion at the
International Astronomical Union in the summer of 2006. Astronomers
held a debate over the meaning of the term "planet"---specifically
whether or not Pluto and the other large KBO's should be placed in a
separate category. In the end, the IAU voted to create a new category
of "dwarf planet" for these latter objects but was then forced
to add the asteroid Ceres for consistency. All this was handled very
clumsily, and it generated needless controversy. It turns out many
non-astronomers were fond of Planet Pluto.
Even before the discovery of Pluto, we had already known of many
small, rocky objects in separate orbits around the Sun---the
"asteroids." Now, we know about many similar, but icy, objects.
Sensible designations for these types, above some threshold in size,
are as "rock dwarf planets" and "ice dwarf planets."
Reading for this lecture:
Seeds, Chapters 23 and 24
Study Guide 20
Reading for next lecture:
Seeds, Chapter 25
Study Guide 21
Web Links:
Last modified
April 2008 by rwo
Text copyright © 1998-2008 Robert W. O'Connell. All
rights reserved. These notes are intended for the private,
noncommercial use of students enrolled in Astronomy 121 at the
University of Virginia.